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Energy and Power Engineering, 2013, 5, 393-397 doi:10.4236/epe.2013.54B076 Published Online July 2013 (http://www.scirp.org/journal/epe) Analysis on the Characteristics of Wind Power Output in Hainan Power Gr i d* Jianfeng Wang, Dongmei Zhao College of Electrical and Electronic Engineering, North China Electric Power University, Beijing, China Email: wjfwjfcool@126.com Received March, 2013 ABSTRACT It is of great importance to study the characteristics of wind power output for the healthy and secure & stable of power grid. Based on the actual operating data, th e probability distribution of the power fluctuations of the wind farm in Hai- nan and the variation of wind power annual, seasonal, daily active output is analyzed. The study showed that Hainan Province has obvious seasonal variation of wind power output characteristics, higher levels of output of the year gener- ally in winter or summer, spring and autumn to contribute small. The av erag e wind power output will contribute to “low day and high night”, with certain peaking capacity. Shorter time scales, changes in the wind power to smaller amount, not to bring too much impact on system operation, while a long time fluctuations affect the scheduling and running on the grid. Keywords: Wind Power; Power Fluctuation; Probability Distribution 1. Introduction With the growing energy and environmental problems, the development of new energy has been a concern around the globe. China has a vast coastline of wind en- ergy resources are widely distributed and relatively rich areas are mainly concentrated in the southeast coast and nearby islands and the northern. In addition, inshore and offshore wind energy resources are very rich [1]. The new energy is one of the pillar industries in recent years to focus on supporting the development of Hainan, Hainan wind power has been rapid development. As of the end of June this year, Hainan new energy installed capacity of 249.5 MW wind power project to dominate. Last year, Hainan wind power generation of 270 million kWh. Because of intermittent, randomness and volatility characteristics of wind, with the rising proportion of wind power installed capacity proportion in the system, the impact on security, stability and economic operation of the power system will cannot be ignored[2,3]. Wind power output change by a variety of geographical and climatic factors. Usually only by the statistics and analy- sis of a large number of actual data, can we get the varia- tion of the wind power in particular areas. Therefore, based on the actual operating data of Hainan several wind farms from 2011 to 2012, variation of wind power annual, seasonal, daily active output is analyzed. Further with the probability distribution method, the fluctuations of wind power are quantitative analyzed, as well as the impact on Hainan power grid. 2. Overview of Wind Power in HAINAN Hainan Island is located in northern margin of tropical, with tropical monsoon maritime climate. Winter prevail- ing northeast monsoon and prevailing southwest mon- soon in the summer, sometimes blowing southeast mon- soon and many tropical cyclones occurs. The wind en- ergy resources which can be developed and used are mainly distributed in th e coastal areas, offshore areas and some inland mountainous area. Off the coast of Hainan is rich in wind energy re- sources, and the average wind speed in most parts is be- tween 4.3 m/s to5.2 m/s. As of the end of 2012, the Hai- nan power gr id has b een pu t into operatio n in w ind f arms in six, the total installed capacity of 303MW, accounting for about 7.23% of the installed capacity of Hainan province. The six grid wind farms are Wenchang wind farm, E’man wind farm, Gancheng wind farm, Sigeng wind farm, Gaopai wind farm and Dongfang wind farm, as shown in Figure 1. The capacity of Dongfang wind farm is very small, and Gaopai just put into operation in the end of the yea r, in th is pap er, the f irst fou r wind f arm will be the research focus. *The National High Technology Research and Development of China 863 Program ( 2012AA050201). Copyright © 2013 SciRes. EPE J. F. WANG, D. M. ZHAO 394 Figure 1. Diagram of wind power in Hainan. 3. Wind Power Output Fluctuation Analyses 3.1. Output Level under Different Years Over a period of time, the wind power output level is constantly in random fluctuations, it is difficult to accu- rately predict, therefore, need to select an indicator to study the laws of statistics. Wind power annual utiliza- tion hours [4], also known as Equivalent full load power generation hours, Refers to the ratio of the actual gener- ating capacity of wind power equipment in the year with annual generating capacity of the power generation equipment running at rated power. Statistics Hainan wind farm operating data in the past two years, the annual uti- lization hours is about 1433 ~ 2340 h, the average value of 2000h. Annual utilization hours of wind power af- fected by multiple factors: 1) the impact of meteorologi- cal factors such as wind conditions, climate, natural dis- asters, etc; 2) wind turbine failure rate, reliable operation time of the unit; 3) the transmission, substation capacity constraints of wind farm area; 4)the electric field losses, transformer, line losses, and other auxiliary power con- sumption. Wind power annual utilization hours can evaluate the level of efficiency in the use of the wind farm, the level of annual utilization hours reflect the relative size of the level of wind speed from the other side in different years. Figure 2 shows, the average wind speed of each region in 2012 is basically lower than 2011. 3.2. Wind Power in Different Seasons and Months The wind speed of an area is largely influenced by the local climate, wind energy resources of monsoon climate region shows apparent regularity in the long-term within the one-year cycle. Active power and capacity factor [5] was chosen as indicators in the Statistics of the output data of the Hainan four wind farms in 2011 and 2012. The results are shown in Figure 3. In 2011 and 2012, the maximum outp ut occurs in Jan- uary and June, with the value 83.3MW and 56.5MW respectively; Minimum output occurs in August and September, 14.8 MW and 22.7 MW respectively. The seasonal maximum peak-to-valley was 68.5 MW and 33.8 MW, accounting for 37.18% and 18.31% of the wind turbine total installed capacity. From the wind power output curves in these two years we can find, generally the largest wind power output appear in the November, December, January, Under the influence of the winter monsoon, Hainan have a greater average wind speed; In the summer, around June, will also appear larger wind, which is related to the impact of the monsoon, and tropical cyclones; spring and autumn wind is small generally. Figure 4 shows annual capacity factor curve in the Wenchang, E’man, Gancheng and Sigeng wind farm in 2011. The curve shows, in the winter, the output of all the wind farms have reached the peak level of the year; Figure 2. Annual utilization hours in different wind farms. Figure 3. The total power of the four wind farms in each month. Figure 4. Annual capacity factor curve in the four wind farms in 2011. Copyright © 2013 SciRes. EPE J. F. WANG, D. M. ZHAO 395 in spring and autumn, wind power output is lower; in the summer, different wind farm have different variation. The geographic distance between Gancheng wind farm and Sigeng wind farm is very near, at the west of Hainan Island, has a similar law for the wind power output fluc- tuations. The curves present bimodal characteristics, winter and summer wind power output is high, while spring and autumn to contribute significantly lower, which exhibit significant characteristics of the monsoon. On the other hand, Wenchang and E’man, at the north of Hainan, have a different variation rule. In winter, wind speed and wind power capacity factor are much higher than other periods, in spring, summer and autumn wind is low, and relatively little change, Curve shows unimodal characteristics. 3.3. Wind Power Output Changes in One Day For power systems, wind power is an uncontrollable power source, the increase in power output of wind pow- er, means that the system equivalents loads is relatively small, and further affect daily open formulation and ad- justment of the shutdown plan of the power system. Therefore, it is necessary to study wind power output variation in 24 hours. With the active output data of wind farms in Hainan in 2012 as the foundation, the variation of the capacity fac- tor of each power plant in one day is calculated, as shown in Figure 5. It can be found in a wide range of areas in Hainan , the capacity factor of wind farms in 24 hours with the same regularity. Wind power output level is low in the night and the morning, and little change; Afternoon, the wind power output level is increasing, and the peak generally appear in the 14:00 to 17:00. We can find that wind power output of Hainan, which is unlike in inland areas of significant anti-peaking[6] characteristics presents the characteristics of “low day and high night” and has cer- tain support and added effect to peak load regulation in power system, on the other hand, it is also conducive to the elimination of the grid for wind power. In the men- tioned four wind farm, E’man, Gancheng Sigeng wind power output shows obvious fluctuations trend in one day, the peak output level can reach twice of the night, while power output is more tend to steady in Wenchang, only a slight increase in the afternoon. In order to study how the wind farm daily output curves changes under different seasons, E’man wind farm is made as an example for analysis on daily output level in each season, as shown in Figure 6. E’man wind farms wind power output has almost the same change trend in different season, showed a single peak characteristic, which usually appear at 14:00 to 17:00, the affection of the seasonal variation on wind power output is mainly reflected in the size of the spe- cific values. Clearly,wind power capacity factor is basic above 0.4 in winter, Indicating that higher utilization efficiency in winter; While in spring, for a very long time, the wind power capacity factor is less than 0.2. 4. Probability Distribution of Wind Power 4.1. Probability Distribution of Wind Speed The distribution characteristics of wind speed generally shows positive skewness, Weibull distribution [7, 8] is generally considered as a suitable probability density function for the wind speed statistical description. The Weibull distribution is a single peak distribution function cluster, which has two parameters. Its probability density function can be expressed as: 1 () exp kk kx x px cc c (1) where, k is called the shape parameter, c called the scale parameter. There are a variety of methods to estimate parameters of the Weibull distribution, which is chosen depending on the wind speed statistics. Three methods are com- monly used [9]: Least squares method, mean and vari- ance estimation method, minimum error approximation method. Figure 5. Wind power capacity factor in E’man, Gancheng Sigeng and Wenchang wind farm in 24 h. Figure 6. Wind power capacity factor in E’man in each season. Copyright © 2013 SciRes. EPE J. F. WANG, D. M. ZHAO 396 According to the statistics of wind sp eed data in 2012, combined with the second method, the calculated wind speed distribution parameters are as follows in Table 1: 4.2. Probability Distribution of Wind Power Fluctuations At present, the quantitative analysis o f the characteristics of wind power fluctuations is few,the probability dis- tribution of the field is also not very mature. The normal distribution can be used to describe the distribution of the first-order differential sequence of wind power [10, 11] proposed an improved t-distribution to describe the min- ute level power fluctuation. The probability distribution of the power differential sequence has an important role to researcher like wind power forecast, wind farms equivalents modeling and so on, so following this de- tailed study: In order to quan tify the power flu ctuations of the wind power, this article refers to two numerical feature amounts to describe the first-order differential sequence of wind power. Assuming that as the wind power of a wind farm at a certain moment, where is an n-dimensional vector, is number of the wind farm units, the average of wind power is PP nP, and using the standard deviation of wind power ou tput as quantita- tive indicators to describe the amplitude of the wind power fluctuation. S 2 1 1( n i i SP n )P (2) Assuming that is to describe the probability of oc- currence of the first-order differential sequence of wind power at different amplitude range [12]. The following formula is: T / p TN N (3) where: p N is the number of occurrences of a certain range of first-order differential sequence, is the to tal number of wi nd power di ff erenti a l sequen ce. N Statistical analysis is to used on Gancheng wind farm actual operating data of one day in2011,installed ca- pacity of 49.5 MW. The distribution of the amplitude of power fluctuation at different time scales (10 s, 1 min, 15 min, 1 h) is shown in Fig u r e 7. Table 1. Wind speed probability distribution parameters in four wind farms. Wind farm Reference height/m average wind speed/(m/s-1) c k E’man 65 6.24 6.12 2.01 Gancheng 65 6.74 5.99 1.63 Sigeng 65 6.12 6.09 2.01 Wenchang 65 6.38 6.14 1.97 Figure 7. Distribution of the amplitude of power fluctuation at different time scales. Table 2. Wind power maximum, and standard of the first-order differential sequence. Time scale 10s 1min 15min 1h Power fluctuations maximum (MW) 0.871 1.875 6.698 6.564 Standard deviation (MW) 0.1456550.400795 1.8723483.588958 At 1min, 15min scale, the probability of the distribu- tion in 0.01pu is 85.25% and 76.0%, respectively; at 10s-15min scale, the probability of the fluctuations of wind power in 0.01pu is almost 100%. With increased sampling time scale, the magnitude of the wind power fluctuations increases, the distribution area of power fluctuations will be more widely. Table 2 from the perspective of the active wind power fluctuation maximum value and the standard deviation, indicating that wind power fluctuations grows with the larger time scale. In the very small time scale, power fluctuations is a smaller amount, does not bring too much impact on the system operation; However, when the size of the grid- connected wind power increasing and wind power pe- netration is high, which will cannot be ignored. The short-term fluctuations affect system infrequency modu- lation, and long-term fluctuations have effect on dispatch- ing and operation of power system. 5. Conclusions Based on Hainan wind farm actual operating data, from the two aspects of the time scale and th e probability den- sity distribution, in this paper, the wind power output in different situations are compared and studied, the con- clusion is as follows: 1) In Hainan, wind farms are mainly located on the west coast and Wenchang, belongs to the offshore wind power; the annual utiliz ati on hours i s about 1433 ~ 234 0 h, the average value of 2000 h, wind energy resources are relatively abundant. 2) The output of wind power has obvious seasonal Copyright © 2013 SciRes. EPE J. F. WANG, D. M. ZHAO Copyright © 2013 SciRes. EPE 397 variation characteristics: in winter, wind power output is at the peak, and there is a clear correlation; the output of spring an d fall of eac h wind farm is low; 3) Unlike inland wind power’s "high day and low night" feature, each wind farm, in every season, the wind power output is basically the same, peak generally appear in the afternoon from 2 o'clock to five o'clock, showed a single peak characteristics conducive to the system peaking wind power consumption; 4) Shorter time scales, changes in the wind power to smaller amount, not to bring too much impact on system operation, long time fluctuations affect the scheduling and running on the grid, the need for furthe r res ea rch. REFERENCES [1] J. F. Li, “China Wind Power Outlook 2012,” Beijing: China Environmental Science Press, 2012. [2] W. Y. Li, B. H. Zhang and Bagen, “Reliability Impacts of Large Scale Utilization of Wind Energy on Electric Power Systems,” Proceedings of the CSEE, Vol. 28, No. 1, 2008, pp.100-105. 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